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    Flow Boundaries in Random-Flight Dispersion Models: Enforcing the Well-Mixed Condition

    Source: Journal of Applied Meteorology:;1993:;volume( 032 ):;issue: 011::page 1695
    Author:
    Wilson, John D.
    ,
    Flesch, Thomas K.
    DOI: 10.1175/1520-0450(1993)032<1695:FBIRFD>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Lagrangian stochastic (LS) dispersion models often use trajectory reflection to limit the domain accessible to a particle. It is shown how the well-mixed condition (Thomson) can he expressed in the Chapman-Kolmogorov equation for a discrete-time LS model to provide a test for the validity of a reflection algorithm. By that means it is shown that the usual algorithm (perfect reflection) is exactly consistent with the wmc when used to bound Gaussian homogeneous turbulence, but that no reflection scheme can satisfy the wmc when applied at a location where the probability distribution for the normal velocity is asymmetric, or locally inhomogeneous. Thus, there is no well-mixed reflection scheme for inhomogeneous or skew turbulence.
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      Flow Boundaries in Random-Flight Dispersion Models: Enforcing the Well-Mixed Condition

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4147260
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    contributor authorWilson, John D.
    contributor authorFlesch, Thomas K.
    date accessioned2017-06-09T14:04:38Z
    date available2017-06-09T14:04:38Z
    date copyright1993/11/01
    date issued1993
    identifier issn0894-8763
    identifier otherams-11973.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4147260
    description abstractLagrangian stochastic (LS) dispersion models often use trajectory reflection to limit the domain accessible to a particle. It is shown how the well-mixed condition (Thomson) can he expressed in the Chapman-Kolmogorov equation for a discrete-time LS model to provide a test for the validity of a reflection algorithm. By that means it is shown that the usual algorithm (perfect reflection) is exactly consistent with the wmc when used to bound Gaussian homogeneous turbulence, but that no reflection scheme can satisfy the wmc when applied at a location where the probability distribution for the normal velocity is asymmetric, or locally inhomogeneous. Thus, there is no well-mixed reflection scheme for inhomogeneous or skew turbulence.
    publisherAmerican Meteorological Society
    titleFlow Boundaries in Random-Flight Dispersion Models: Enforcing the Well-Mixed Condition
    typeJournal Paper
    journal volume32
    journal issue11
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1993)032<1695:FBIRFD>2.0.CO;2
    journal fristpage1695
    journal lastpage1707
    treeJournal of Applied Meteorology:;1993:;volume( 032 ):;issue: 011
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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